Orbital forcing of ice sheets during snowball Earth

The snowball Earth hypothesis—that a runaway ice-albedo feedback can cause global glaciation—seeks to explain low-latitude glacial deposits, as well as geological anomalies including the re-emergence of banded iron formation and “cap” carbonates. One of the most significant challenges to snowball Ea...

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Detalles Bibliográficos
Autores principales: Mitchell, Ross N., Gernon, Thomas M., Cox, Grant M., Nordsvan, Adam R., Kirscher, Uwe, Xuan, Chuang, Liu, Yebo, Liu, Xu, He, Xiaofang
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8263735/
https://www.ncbi.nlm.nih.gov/pubmed/34234152
http://dx.doi.org/10.1038/s41467-021-24439-4

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8263735/
https://www.ncbi.nlm.nih.gov/pubmed/34234152
http://dx.doi.org/10.1038/s41467-021-24439-4

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